{"title":"Diversity of La Niña onset","authors":"Xiao Pan, Tim Li","doi":"10.1038/s41612-025-01141-6","DOIUrl":null,"url":null,"abstract":"<p>Three La Niña onset types were identified by the K-means cluster analysis of equatorial sea surface temperature anomaly evolutions during the past 111 years (1910–2020). The first type is characterized by a slow basin-wide transition from a neutral year to La Niña, driven by tropical North Atlantic (TNA) warming, which induced anomalous easterlies in the equatorial western Pacific through atmospheric Kelvin wave responses. The easterly anomalies initiate a cooling by triggering upwelling oceanic Kelvin waves, shoaling the thermocline, and strengthening the westward zonal currents. The second and third types are a transition from a central Pacific (CP) and a super eastern Pacific (EP) El Niño to La Niña. The former is attributed to the CP El <span>\\({\\rm{Ni}}\\tilde{{\\rm{n}}}{\\rm{o}}\\)</span> induced anomalous easterlies in EP that strengthened local surface latent heat flux and anomalous upwelling, whereas the latter is attributed to a substantially shoaling of ocean thermocline associated with the discharge of the preceding super El <span>\\({\\rm{Ni}}\\tilde{{\\rm{n}}}{\\rm{o}}\\)</span>. These characteristics differentiate diversified types of La Niña onset.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"13 1","pages":""},"PeriodicalIF":8.5000,"publicationDate":"2025-07-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"npj Climate and Atmospheric Science","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1038/s41612-025-01141-6","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
Three La Niña onset types were identified by the K-means cluster analysis of equatorial sea surface temperature anomaly evolutions during the past 111 years (1910–2020). The first type is characterized by a slow basin-wide transition from a neutral year to La Niña, driven by tropical North Atlantic (TNA) warming, which induced anomalous easterlies in the equatorial western Pacific through atmospheric Kelvin wave responses. The easterly anomalies initiate a cooling by triggering upwelling oceanic Kelvin waves, shoaling the thermocline, and strengthening the westward zonal currents. The second and third types are a transition from a central Pacific (CP) and a super eastern Pacific (EP) El Niño to La Niña. The former is attributed to the CP El \({\rm{Ni}}\tilde{{\rm{n}}}{\rm{o}}\) induced anomalous easterlies in EP that strengthened local surface latent heat flux and anomalous upwelling, whereas the latter is attributed to a substantially shoaling of ocean thermocline associated with the discharge of the preceding super El \({\rm{Ni}}\tilde{{\rm{n}}}{\rm{o}}\). These characteristics differentiate diversified types of La Niña onset.
期刊介绍:
npj Climate and Atmospheric Science is an open-access journal encompassing the relevant physical, chemical, and biological aspects of atmospheric and climate science. The journal places particular emphasis on regional studies that unveil new insights into specific localities, including examinations of local atmospheric composition, such as aerosols.
The range of topics covered by the journal includes climate dynamics, climate variability, weather and climate prediction, climate change, ocean dynamics, weather extremes, air pollution, atmospheric chemistry (including aerosols), the hydrological cycle, and atmosphere–ocean and atmosphere–land interactions. The journal welcomes studies employing a diverse array of methods, including numerical and statistical modeling, the development and application of in situ observational techniques, remote sensing, and the development or evaluation of new reanalyses.